Mobilization of old terrestrial carbon caused by permafrost thawing, sea-level rise and ice-sheet melting during the last deglaciation

The last deglaciation was characterized by rising concentrations in atmospheric CO2 (CO2atm) and a decrease in its radiocarbon content (∆14Catm). Mobilization of 14C-depleted terrestrial organic carbon, which was previously frozen in extensive boreal permafrost soils, might have contributed to both...

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Bibliographic Details
Main Authors: Mollenhauer, Gesine, Winterfeld, Maria, Meyer, Vera, Köhler, Peter, Dummann, Wolf, Grotheer, Hendrik, Lembke-Jene, Lester, Hefter, Jens, McIntyre, Cameron, Wacker, Lukas, Haghipour, Negar, Gersonde, Rainer, Tiedemann, Ralf
Format: Conference Object
Language:unknown
Published: 2018
Subjects:
Ice
Online Access:https://epic.awi.de/id/eprint/47461/
https://hdl.handle.net/10013/epic.4bd16db3-994e-4b37-8bfd-838adad294eb